Results 31 to 40 of about 896 (145)
High (ultrahigh) pressure metamorphic terrane rocks as the source of the detrital garnets from the Middle Jurassic sands and sandstones of the Cracow Region (Cracow- Wieluń Upland, Poland) [PDF]
, 2012 The Middle Jurassic (Upper Bathonian/Lower Callovian) sands and sandstones of the Cracow–Wieluń Upland contain detrital garnets with high contents of the pyrope molecule (30–73 mol %).
Aubrecht, Roman +3 more
core +1 more source
Deep structure of the Pieniny Klippen Belt in Poland
Swiss Journal of Geosciences, 2019 An interpretation of the deep structure of the Pieniny Klippen Belt in Poland is presented, utilizing a high-resolution deep seismic reflection survey. The studied profiles reach a depth of around 23 km. The seismic lines depict the structure and mutual relationships between the main domains analyzed—the Central Carpathians (CC), the Pieniny Klippen ...
Jan Golonka +6 more
openaire +1 more source
Paleopiezometry – the new investigation method applied to the Penninic suture zone in comparison to the Meliata-Hallstatt suture zone [PDF]
Acta Montanistica Slovaca, 2016 The method of paleopiezometry reveals new pleopiezometric data of differential stresses within the calcite veins in outcrops with developed fold structure near the village of Chmeľnica – eastern sector of the Pieniny Klippen Belt – PKB(the Inner ...
Barbora Zákršmidová +2 more
doaj +1 more source
Geologica Carpathica, 2018 The Manín Unit represents a transitional tectonic element between the Central Western Carpathians and the Pieniny Klippen Belt. The overall map-view structure of the Manín Unit is dominated by elliptical antiforms composed of comparatively competent ...
Plašienka Dušan +2 more
doaj +1 more source
Thin‐Sheet Inversion Modeling of Geomagnetic Deep Sounding Data Using MCMC Algorithm
International Journal of Geophysics, Volume 2013, Issue 1, 2013., 2013 The geomagnetic deep sounding (GDS) method is one of electromagnetic (EM) methods in geophysics that allows the estimation of the subsurface electrical conductivity distribution. This paper presents the inversion modeling of GDS data employing Markov Chain Monte Carlo (MCMC) algorithm to evaluate the marginal posterior probability of the model ...
Hendra Grandis +3 more
wiley +1 more source
Annales Societatis Geologorum Poloniae, 2015 Planktonic foraminifera, calcareous dinocysts and nannofossils have been identified in thin sections of the “spotted limestone”, exposed in the Grajcarek Stream at Szlachtowa and assigned to the Pieniny Limestone Formation in the Magura Succession, Pieniny Klippen Belt (southern Poland).
Wójcik-Tabol, Patrycja +1 more
openaire +4 more sources
Výskyt spodnokriedových magmatických hornín medzi Podbrančom a Myjavou [PDF]
Geologické práce. Správy, 2020 Occurrences of magmatic rocks were identifid north of the settlement Belanskovci (part of Myjava town), on the ridge of the elevation point 464 m a. s. l. east of the settlement Podzámok (part of the Podbranč village).
Tamás Csibri +2 more
doaj
Geological setting and lithological inventory of the Czarna Woda conglomerates (Magura Nappe, Polish Outer Carpathians) [PDF]
, 2020 During the late Oligocene to early Miocene the residual Magura Basin was located along the front of the Pieniny Klippen Belt (PKB). This basin was supplied with clastic material derived from a south-eastern direction. In the Małe (Little) Pieniny Mts. in
Olszewska, Barbara +2 more
core +1 more source
Geologica Carpathica, 2019 Coral bioherms of the Vršatec Limestone that formed massive, several tens of meters thick complexes during the Jurassic were important sources of carbonate production, with carbonate sediment exported to deeper parts of the Pieniny Klippen Basin (Western
Ivanova Daria K. +4 more
doaj +1 more source
Mineralia SlovacaThe Pieniny Klippen Belt is characterized by the block-in-matrix fabric with Jurassic to Lower Cretaceous rigid klippen embedded in less competent Upper Cretaceous flysch and marlstone matrix.
Ondrej Pelech +2 more
doaj +1 more source